Scientists have identified a water-loss mechanism on Venus that could explain how the once water-rich world became completely parched.
In the newly identified process, linked to a previously overlooked molecule high in Venus' atmosphere, water escaped Venus at double the rate previously estimated. As faster water loss means less time is needed to boil away the planet's water reservoir, scientists say Venus may have harbored oceans — and potentially habitable conditions — for longer than previously thought before the drying process began.
